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结晶作用

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Life originated and evolved as a unified whole,an integrated consequence of crystallization processes in complex hydrocarbon syst ems,rather than result of coincidence of random events and combination of geneti cally different components.

生命作为统一的整体,作为复杂碳氢体系结晶作用的完整结果产生和演化,而不是偶然事件巧合或不同成因组分结合的结果。

Analysis of structure and fabric shows that the formation mechanism of new fabrics in these experiments is principally recrystallization.

结构和组构分析表明,新组构的形成机制主要是再结晶作用

However, the influences of electric field on the recrystallization and recrystallization texture development are not clear.

研究电场作用下的再结晶过程及再结晶织构的演变规律,不但可以加深对再结晶形成机制和电场作用机理的理解,而且可以为再结晶织构的调控提供一条有效途径。

The magmatite in the area consist mainly of granite, monzonitic granite, syenogranite and acid volcanics.

研究区出露的岩浆岩主要为花岗岩、二长花岗岩、正长花岗岩和酸性火山岩,岩石化学成分上以富铝钾、贫镁铁,且经历了较大的分离结晶作用为特征。

Combined crystallization kinetics analysis obtained via rheometry and morphological observation of crystals growth performed on POM, two different mechanisms of shear-enhanced crystallization for PP/ grafted MWCNTs composites were suggested:(1) at low temperature, strong heterogeneous nucleation plays a dominant role on the. crystallization behavior, which would be saturated at a higher filler content, and the effect of shear-enhanced crystallization was weak;(2) at high temperature, the effect of heterogeneous nucleation was substantially depressed, and the crystallization of the composite was obviously accelerated by pre-shear and the thread-like crystallites were generated earlier than the spherulites.

结合流变测试结果和热台偏光显微镜观察的结晶形貌发展过程,对于PP/G—MWCNTs体系得到了两个不同的剪切影响机理:(1)在低温条件下,强烈的异相成核作用对结晶行为的影响占主导优势,而剪切作用对结晶的影响十分微弱,同时,在填料含量较高是,异相成核作用具有饱和性;(2)在高温条件下,异相成核作用被抑制,复合体系的结晶主要受到预剪切作用的影响,并且纤维状晶体较球晶更易生成。

Geochemical characteristics indicate S-type granites and volcanic rocks depleted in sodium and enriched in potassium, with 62.42%~78.02% w(SiO2), 7.66%~9.13% w(K2O+Na2O), 1.18~2.62 w(K2O)/w(Na2O), and Rittmann index δ of 1.67~3.78. They are enriched in LREE with an average LREE/HREE ratio of 10.94×10-6, and generally depleted Eu with an minimum δEu less than 0.31 especially in the ignimbrite and biotite granite, which have experienced a significant process of separation and crystallization of plagioclases.ΣREE at the main stage of the magmatic activity decreases with time.

地球化学特征显示矿区火山——侵入岩属于贫钠富钾的S型花岗岩,其w(SiO2)值为62.42%~78.02%、w(K2O +Na2O)值为7.66%~9.13%、w(K2O)/w(Na2O)比值为1.18~2.62、里特曼指数δ为1.67~3.78;矿区岩石LREE/HREE比值平均为10.94×10-6,属于轻稀土富集型;Eu普遍亏损,特别是熔结凝灰岩、黑云母花岗岩δEu<0.31,表明经历了显著的斜长石的分离结晶作用;自早至晚主阶段岩浆活动稀土总量逐渐降低。

Low concentration of compatible elements in all the rocks indicates the magmas experienced different extent of differentiation crystallization.

各期次玄武岩的相容元素丰度较低,表明岩浆发生过不同程度的分离结晶作用

This paper has investigated the microstructures, quartz fabrics, and mineral chemistry of mylonites from the ductile shear zone of the granite-greenstone belt in Seerteng area, Inner Mongolia. Synthetic analyses reveal that the mylonites underwent four evolutionary processes of deformation and metamorphism, such as lower-amphibolite facies regional metamorphism, retrograde epidote-amphibolite facies metamorphism and deformation, progressive recrystallization and retrograde greenschist facies metamorphism and deformation.

通过对色尔腾山地区花岗绿岩带中韧性剪切带的糜棱岩显微构造、石英组构、矿物化学等综合分析,发现该区糜棱岩在经历了低角闪岩相区域变质及绿帘角闪岩相退变质变形之后,发生了不均匀进变质重结晶作用及中低绿片岩相退变质变形等几个演化阶段。

Carbonate rocks are susceptible to later recrystallization during deep burial, and can isotopically re-equilibrate with higher-temperature fluids depending upon the water/rock ratios and the isotopic composition of the fluids.

碳酸盐岩在深埋过程中很容易被后期的重结晶作用影响,并且在高温流体的加入时发生同位素的分馏,这种分馏与水/岩比率以及流体同位素的组成相关。

The molecular motion of amorphous region at high-frequency was found to be hardly affected during the stretching processes. In summary, elongation has created major but different influences on the morphology and molecular motion of the aforementioned four series of polymeric elastomers. For those elastomers like natural rubber and poly , elongation has induced crystallization of the noncrystalline or the soft segments. The crytallinitiy and the crystal thicknesses increase monotonously during the course of the stretching; On the other hand, the stretching processes for those semicrytalline copolymers like EMA and POE are rather complex, including the formation of crystal at relatively low λand the destruction of the crystal at the utmost λ. It revealed that stretching process has resulted in a decreasing of the thicknesses and a shortening of 〓C T〓s for the orthorhombic crystalline components.

拉伸对上述四个弹性体体系的聚集态结构都产生了很大影响,但是影响的程度和内容因体系而不同,对于本身存在着化学交联或者是物理交联的体系而言,拉伸导致了其中本来难以结晶组分的结晶,且结晶度随着拉伸比增加而增加,与此同时,体系结晶的晶片厚度也会逐渐增加;而对于结晶性共聚物体系,如EMA和POE,结晶区本来起到了物理交联的作用,在这种情况下拉伸的影响变得比较复杂,拉伸对于不同晶型的影响有所不同,在拉伸比较低的情况下体系总体的结晶度会有所增加,说明有新的结晶产生,当接近或达到断裂伸长比时,体系的结晶度会突然降低,含量占优的结晶会被拉伸所破坏,含量较低的结晶在整个拉伸过程中受的影响较小。

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